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Six Major Types of Crystal Formation Shapes

Crystals are the basic building blocks from which minerals are made. These crystals have their own properties and can be described in terms of their structure and symmetry to fit into one of six crystal systems. Each crystal that fits into a particular system will share characteristics, specifically in terms of symmetry, with the other crystals in that category. It is sometimes possible to ascertain the system a crystal fits into just by looking at it. This is only true if the crystal is a very good example of its category.

Cubic
- The cubic crystal system is also known as isometric. As the name suggests, crystals in this system are shaped like cubes, with six faces set at 90 degree angles to each other. The three axes of symmetry, called crystallographic axes, are all perpendicular to each other and of equal lengths. An example of a mineral with crystals that fit into this system is halite, otherwise known as salt.
Tetragonal
- Crystals in the tetragonal system are shaped like cuboids. This system also has six faces which sit at 90 degrees to each other. The difference between this system and the cubic one is that although the three crystallographic axes are still perpendicular to each other, only two are of the same length. The third is longer, creating the rectangular shape. Zircon is an example of a mineral in this crystal system.
Hexagonal
- Crystals in this system are shaped like hexagonal prisms. Because these crystals have six sides, there is an additional axis. Of the four axes, three are the same length, and are at 60 degrees to one another. The vertical axis is longer than the others and at 90 degrees to the shorter ones. This crystal system is further divided into hexagonal and rhombohedral. Emerald is a gemstone with hexagonal crystals.
Orthorhombic
- Orthorhombic crystals are irregular in shape. They have six sides and three perpendicular axes, but each axis is a different length to the others. A number of minerals are made of crystals that fit into this system, including topaz, peridot and tanzanite.
Monoclinic
- Crystals of the monoclinic system have six sides and three axes. The axes are all of different lengths and two of them, one being the vertical axis, meet at 90 degrees. The third axis is not perpendicular to the other two. Examples of minerals that fit into the monoclinic crystal system are gypsum and feldspar.
Triclinic
- The final crystal system is known as triclinic. Crystals in this system have six sides and three axes of symmetry. None of the axes are equal in length and none are perpendicular to either of the others. Turquoise is an example of a gemstone that fits this crystal system.

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